Paleoenvironmental reconstructions on a (supra-) regional scale have gained attention in
Quaternary sciences during the last decades. In terrestrial realms, loess deposits and …

Loess formation generally involves the four main stages of production, deflation,
transportation, and deposition of loess particles. Traditionally, loesses are classified as …

Original vertical joints (OVJs), which are highly correlated with loess anisotropy, have been
considered a non-tectonic source of extensive erosion, gully development, and landform …

Central Asia (CA) is one of the main loess regions in the world and provides important
information for the understanding of paleoclimate and paleoenvironmental changes …

Abstract In the Carpathian Basin, loess is the most important archive of Quaternary
palaeoclimate evolution, but only in the past two decades systematic and high-resolution …

Loess in Europe is heterogeneous due to differences in paleoenvironmental conditions
during sedimentation and pedogenesis. In many regions of Europe, including southern …

Loess deposits are widely distributed along the mountain piedmonts of Central Asia. The
transport processes and origins of Central Asian loess sediments remain poorly understood …

Thin loess deposits are widespread soil parent materials and important archives for
paleoenvironmental reconstruction. The origin of loess in SW Poland is attributed to the …

Loess deposits in southern Britain contain a record of dust, climate and landscape dynamics
over the last glacial, yet their age and accumulation rate remain poorly known. Furthermore …

Loess, as a terrestrial aeolian deposit, forms extensive landforms over several parts of the
Central Asia, especially in southern Tajikistan. However, the dust dynamics for the loess …